TY - JOUR
T1 - Preparation of Cu-mordenite by ionic exchange reaction under milling
T2 - A favorable route to form the mono-(μ-oxo) dicopper active species
AU - Sainz-Vidal, Arianee
AU - Balmaseda, Jorge
AU - Lartundo-Rojas, Luis
AU - Reguera, Edilso
N1 - Funding Information:
The authors thank Dr. N. Barba, Dr. H. López, Dr. A. Lemus, M. A. Canseco and Lazaro Huerta for the invaluable experimental facility. A.S.-V. thanks CONACyT and IPN (Mexico) for PhD scholarship grants. This study was partially supported by the projects CONACyT- 2009-01-129048 , 2010-117373 , 2011-174247 , I010/296/2012 , 2012-193850 and 2012-154626 .
PY - 2014/2/1
Y1 - 2014/2/1
N2 - Cu-exchanged mordenite samples were prepared using both solid state and aqueous solution ionic reactions. The obtained materials were then characterised from UV-vis, XPS, and TPR data in order to obtain information on the state of copper in the exchanged samples. Three types of copper species were identified, surface clusters of Cu2O, hydrated Cu(II) ions with two slightly different coordination environments, and mono (μ-oxo) dicopper core, [Cu 2O]2+, located in β type channels for samples activated on heating in the presence of oxygen. The formation of this last species, active for the methane conversion into methanol, was found to be particularly favored for the solid state ionic exchange reaction, and it is detected as an intense charge transfer band at 400 nm in the recorded UV-vis spectra and a well-defined peak at 936.34 eV of binding energy in the XPS spectra. The stabilisation of this dicopper core is the main distinctive difference between the exchange reactions in the solid state and in solution. The appearance of this bridged binuclear Cu2+ species was also detected in the recorded TPR profiles. According to the recorded CO2 adsorption isotherms, the ionic exchange process modifies the accessible pore volume but the material preserves its porous features. The ability of that core for the low temperature methane conversion into methanol was confirmed recording chromatographic profile at different temperatures.
AB - Cu-exchanged mordenite samples were prepared using both solid state and aqueous solution ionic reactions. The obtained materials were then characterised from UV-vis, XPS, and TPR data in order to obtain information on the state of copper in the exchanged samples. Three types of copper species were identified, surface clusters of Cu2O, hydrated Cu(II) ions with two slightly different coordination environments, and mono (μ-oxo) dicopper core, [Cu 2O]2+, located in β type channels for samples activated on heating in the presence of oxygen. The formation of this last species, active for the methane conversion into methanol, was found to be particularly favored for the solid state ionic exchange reaction, and it is detected as an intense charge transfer band at 400 nm in the recorded UV-vis spectra and a well-defined peak at 936.34 eV of binding energy in the XPS spectra. The stabilisation of this dicopper core is the main distinctive difference between the exchange reactions in the solid state and in solution. The appearance of this bridged binuclear Cu2+ species was also detected in the recorded TPR profiles. According to the recorded CO2 adsorption isotherms, the ionic exchange process modifies the accessible pore volume but the material preserves its porous features. The ability of that core for the low temperature methane conversion into methanol was confirmed recording chromatographic profile at different temperatures.
KW - Adsorption
KW - Copper μ-oxo dimer
KW - Ionic exchange
KW - Solid state reaction
KW - Zeolite
UR - http://www.scopus.com/inward/record.url?scp=84889857839&partnerID=8YFLogxK
U2 - 10.1016/j.micromeso.2013.11.009
DO - 10.1016/j.micromeso.2013.11.009
M3 - Artículo
SN - 1387-1811
VL - 185
SP - 113
EP - 120
JO - Microporous and Mesoporous Materials
JF - Microporous and Mesoporous Materials
ER -